Official Series Description


Lab Data Summary

Aggregate lab data for the ROUNDOR soil series. This aggregation is based on all pedons with a current taxon name of ROUNDOR, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to ROUNDOR were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
4492P031589MT0391304Roundor7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5369453,-113.1630554

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ROUNDOR soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ROUNDOR series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the ROUNDOR series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the ROUNDOR series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with ROUNDOR share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the ROUNDOR series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the ROUNDOR series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with ROUNDOR, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing ROUNDOR as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Windham-Kiev-Roundor complex, 4 to 15 percent slopes564D433039575pg4tmt60219631:20000
Roundor loam, 4 to 8 percent slopes44C22071444264v8xmt62119971:24000
Roundor loam, 8 to 15 percent slopes44D14091444274v8ymt62119971:24000
Roundor loam, 15 to 35 percent slopes44E9011444284v8zmt62119971:24000
Roundor-Lap complex, 15 to 35 percent slopes440E7381444114v8fmt62119971:24000
Roundor loam, 2 to 4 percent slopes44B5071444254v8wmt62119971:24000
Roundor-Lap complex, 8 to 15 percent slopes440D1311444104v8dmt62119971:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes, foothills945C156425232354z2wmt62420211:24000
Windham-Kiev-Roundor complex, 4 to 15 percent slopes564D582485183pg4tmt62420211:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes, foothills945E5631768364z2xmt62420211:24000
Windham-Kiev-Roundor complex, 4 to 15 percent slopes564D4812392825pg4tmt6321:24000
Roundor-Maiden complex, 4 to 15 percent slopes, very bouldery458D5624862602pg4ymt6321:24000
Roundor-Lap complex, 8 to 15 percent slopes440D29817029551v521mt63520061:24000
Roundor loam, 15 to 35 percent slopes44E23417029501v51wmt63520061:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes445C517824963772pqkbmt63720141:24000
Windham-Kiev-Roundor complex, 4 to 15 percent slopes564D3876639214pg4tmt63720141:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes445E282825173572q9zvmt63720141:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes, foothills945C25291480834z2wmt63720141:24000
Roundor-Maiden complex, 4 to 15 percent slopes, very bouldery458D816816582wdqcmt63720141:24000
Roundor-Cabba complex, 2 to 8 percent slopes845C5841480784z2qmt63720141:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes, foothills945E3211480844z2xmt63720141:24000
Kiev-Roundor loams, 2 to 15 percent slopes184D16902348407cpjymt65719901:24000
Kiev-Roundor-Windham complex, 15 to 45 percent slopes475F8397348676cptmmt65719901:24000
Kiev-Roundor gravelly loams, 2 to 15 percent slopes284D8259348534cpp1mt65719901:24000
Cabba-Roundor-Windham complex, 25 to 60 percent slopes474F4357348673cptjmt65719901:24000
Windham-Kiev-Roundor complex, 4 to 15 percent slopes564D1522995248pg4tmt66620081:24000
Almaholt-Roundor-High loams, 3 to 30 percent slopes2006716314802231lp94wy0411:24000
Roundor-Kiev complex, 25 to 45 percent slopes2115627186262120j6kwy0411:24000
Ridge-Roundor, extremely stony complex, 25 to 45 percents slopes2124720186263320j6ywy0411:24000

Map of Series Extent

Approximate geographic distribution of the ROUNDOR soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .